Unify boundary conditions

Project.toml

@@ -33,5 +33,5 @@ Static = "0.8, 1"
 StaticArrayInterface = "1.5.1"
 StaticArrays = "1"
 StrideArrays = "0.1.28"
-Trixi = "0.14"
+Trixi = "0.15"
 julia = "1.10"

examples/advection/cartesian/elixir_cubed_sphere.jl

@@ -67,7 +67,8 @@ initial_condition_transformed = transform_initial_condition(initial_condition, e
 
 # A semidiscretization collects data structures and functions for the spatial discretization
 semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_transformed, solver,
-                                    source_terms = source_terms_convert_to_linear_advection)
+                                    source_terms = source_terms_convert_to_linear_advection,
+                                    boundary_conditions = boundary_condition_periodic)
 
 ###############################################################################
 # ODE solvers, callbacks etc.

examples/advection/cartesian/elixir_quad_icosahedron.jl

@@ -65,7 +65,8 @@ initial_condition_transformed = transform_initial_condition(initial_condition, e
 
 # A semidiscretization collects data structures and functions for the spatial discretization
 semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_transformed, solver,
-                                    source_terms = source_terms_convert_to_linear_advection)
+                                    source_terms = source_terms_convert_to_linear_advection,
+                                    boundary_conditions = boundary_condition_periodic)
 
 ###############################################################################
 # ODE solvers, callbacks etc.

examples/advection/covariant/elixir_cubed_sphere.jl

@@ -18,8 +18,8 @@ equations = CovariantLinearAdvectionEquation2D(global_coordinate_system = Global
 solver = DGSEM(polydeg = 3, surface_flux = flux_lax_friedrichs,
                volume_integral = VolumeIntegralWeakForm())
 
-# Create a 2D cubed sphere mesh the size of the Earth. For the covariant form to work 
-# properly, we currently need polydeg to equal that of the solver, 
+# Create a 2D cubed sphere mesh the size of the Earth. For the covariant form to work
+# properly, we currently need polydeg to equal that of the solver,
 # initial_refinement_level = 0 (default), and element_local_mapping = true.
 mesh = P4estMeshCubedSphere2D(cells_per_dimension[1], EARTH_RADIUS,
                               polydeg = Trixi.polydeg(solver),
@@ -29,7 +29,8 @@ mesh = P4estMeshCubedSphere2D(cells_per_dimension[1], EARTH_RADIUS,
 initial_condition_transformed = transform_initial_condition(initial_condition, equations)
 
 # A semidiscretization collects data structures and functions for the spatial discretization
-semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_transformed, solver)
+semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_transformed, solver,
+                                    boundary_conditions = boundary_condition_periodic)
 
 ###############################################################################
 # ODE solvers, callbacks etc.

examples/advection/covariant/elixir_quad_icosahedron.jl

@@ -18,7 +18,7 @@ equations = CovariantLinearAdvectionEquation2D(global_coordinate_system = Global
 solver = DGSEM(polydeg = 3, surface_flux = flux_lax_friedrichs,
                volume_integral = VolumeIntegralWeakForm())
 
-# Create a 2D quadrilateral icosahedral mesh the size of the Earth. For the covariant form 
+# Create a 2D quadrilateral icosahedral mesh the size of the Earth. For the covariant form
 # to work properly, we currently need polydeg to equal that of the solver, and
 # initial_refinement_level = 0 (default)
 mesh = P4estMeshQuadIcosahedron2D(cells_per_dimension[1], EARTH_RADIUS,
@@ -28,19 +28,20 @@ mesh = P4estMeshQuadIcosahedron2D(cells_per_dimension[1], EARTH_RADIUS,
 initial_condition_transformed = transform_initial_condition(initial_condition, equations)
 
 # A semidiscretization collects data structures and functions for the spatial discretization
-semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_transformed, solver)
+semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_transformed, solver,
+                                    boundary_conditions = boundary_condition_periodic)
 
 ###############################################################################
 # ODE solvers, callbacks etc.
 
 # Create ODE problem with time span from 0 to T
 ode = semidiscretize(semi, (0.0, 12 * SECONDS_PER_DAY))
 
-# At the beginning of the main loop, the SummaryCallback prints a summary of the simulation 
+# At the beginning of the main loop, the SummaryCallback prints a summary of the simulation
 # setup and resets the timers
 summary_callback = SummaryCallback()
 
-# The AnalysisCallback allows to analyse the solution in regular intervals and prints the 
+# The AnalysisCallback allows to analyse the solution in regular intervals and prints the
 # results
 analysis_callback = AnalysisCallback(semi, interval = 10,
                                      save_analysis = true,
@@ -53,15 +54,15 @@ save_solution = SaveSolutionCallback(interval = 10,
 # The StepsizeCallback handles the re-calculation of the maximum Δt after each time step
 stepsize_callback = StepsizeCallback(cfl = 0.7)
 
-# Create a CallbackSet to collect all callbacks such that they can be passed to the ODE 
+# Create a CallbackSet to collect all callbacks such that they can be passed to the ODE
 # solver
 callbacks = CallbackSet(summary_callback, analysis_callback, save_solution,
                         stepsize_callback)
 
 ###############################################################################
 # run the simulation
 
-# OrdinaryDiffEq's `solve` method evolves the solution in time and executes the passed 
+# OrdinaryDiffEq's `solve` method evolves the solution in time and executes the passed
 # callbacks
 sol = solve(ode, CarpenterKennedy2N54(williamson_condition = false),
             dt = 1.0, save_everystep = false, callback = callbacks)

examples/euler/dry_air/buoyancy/elixir_energy_inertia_gravity_waves.jl

@@ -72,7 +72,7 @@ polydeg = 3
 solver = DGSEM(polydeg = polydeg, surface_flux = surface_flux,
                volume_integral = VolumeIntegralFluxDifferencing(volume_flux))
 
-boundary_conditions = (x_neg = boundary_condition_periodic,
+boundary_conditions = (; x_neg = boundary_condition_periodic,
                        x_pos = boundary_condition_periodic,
                        y_neg = boundary_condition_slip_wall,
                        y_pos = boundary_condition_slip_wall)

examples/euler/dry_air/buoyancy/elixir_gemein_bubble.jl

@@ -52,8 +52,8 @@ end
 
 initial_condition = initial_condition_warm_bubble
 
-boundary_conditions = Dict(:y_neg => boundary_condition_slip_wall,
-                           :y_pos => boundary_condition_slip_wall)
+boundary_conditions = (; y_neg = boundary_condition_slip_wall,
+                       y_pos = boundary_condition_slip_wall)
 
 # Gravity source since Q_ph=0
 source_term = source_terms_geopotential

examples/euler/dry_air/buoyancy/elixir_gemein_nonhydrostatic_gravity_waves.jl

@@ -54,7 +54,7 @@ end
 
 source_term = source
 
-boundary_conditions = (x_neg = boundary_condition_periodic,
+boundary_conditions = (; x_neg = boundary_condition_periodic,
                        x_pos = boundary_condition_periodic,
                        y_neg = boundary_condition_slip_wall,
                        y_pos = boundary_condition_slip_wall)

examples/euler/dry_air/buoyancy/elixir_potential_temperature_inertia_gravity_waves.jl

@@ -50,7 +50,7 @@ polydeg = 3
 solver = DGSEM(polydeg = polydeg, surface_flux = surface_flux,
                volume_integral = VolumeIntegralFluxDifferencing(volume_flux))
 
-boundary_conditions = (x_neg = boundary_condition_periodic,
+boundary_conditions = (; x_neg = boundary_condition_periodic,
                        x_pos = boundary_condition_periodic,
                        y_neg = boundary_condition_slip_wall,
                        y_pos = boundary_condition_slip_wall)

examples/euler/dry_air/buoyancy/elixir_potential_temperature_robert_bubble.jl

@@ -59,7 +59,7 @@ polydeg = 3
 solver = DGSEM(polydeg = polydeg, surface_flux = surface_flux,
                volume_integral = VolumeIntegralFluxDifferencing(volume_flux))
 
-boundary_conditions = (x_neg = boundary_condition_periodic,
+boundary_conditions = (; x_neg = boundary_condition_periodic,
                        x_pos = boundary_condition_periodic,
                        y_neg = boundary_condition_slip_wall,
                        y_pos = boundary_condition_slip_wall)

examples/euler/dry_air/global_circulation/elixir_energy_baroclinic_instability.jl

@@ -200,8 +200,8 @@ equations = CompressibleEulerEnergyEquationsWithGravity3D(c_p = 1004,
 
 initial_condition = initial_condition_baroclinic_instability
 
-boundary_conditions = Dict(:inside => boundary_condition_slip_wall,
-                           :outside => boundary_condition_slip_wall)
+boundary_conditions = (; inside = boundary_condition_slip_wall,
+                       outside = boundary_condition_slip_wall)
 
 polydeg = 5
 surface_flux = (FluxLMARS(340), flux_zero)

examples/euler/dry_air/global_circulation/elixir_potential_temperature_baroclinic_instability.jl

@@ -1,6 +1,6 @@
 # An idealized baroclinic instability test case
 # For optimal results consider increasing the resolution to 16x16x8 trees per cube face.
-# 
+#
 # This elixir takes about 8 hours, using 16 threads of an AMD Ryzen 7 7800X3D.
 #
 # References:
@@ -198,8 +198,8 @@ equations = CompressibleEulerPotentialTemperatureEquationsWithGravity3D(c_p = 10
 
 initial_condition = initial_condition_baroclinic_instability
 
-boundary_conditions = Dict(:inside => boundary_condition_slip_wall,
-                           :outside => boundary_condition_slip_wall)
+boundary_conditions = (; inside = boundary_condition_slip_wall,
+                       outside = boundary_condition_slip_wall)
 
 polydeg = 5
 surface_flux = (FluxLMARS(340), flux_zero)

examples/euler/dry_air/global_circulation/elixir_potential_temperature_held_suarez.jl

@@ -115,8 +115,8 @@ equations = CompressibleEulerPotentialTemperatureEquationsWithGravity3D(c_p = 10
 
 initial_condition = initial_condition_isothermal
 
-boundary_conditions = Dict(:inside => boundary_condition_slip_wall,
-                           :outside => boundary_condition_slip_wall)
+boundary_conditions = (; inside = boundary_condition_slip_wall,
+                       outside = boundary_condition_slip_wall)
 
 polydeg = 4
 surface_flux = (FluxLMARS(340), flux_zero)

examples/euler/dry_air/mountain_flow/elixir_potential_temperature_schaer_mountain.jl

@@ -98,10 +98,10 @@ alpha = 0.03
 xr_B = 20000
 schär_setup = SchärSetup(alpha, xr_B)
 boundary = BoundaryConditionDirichlet(schär_setup)
-boundary_conditions = Dict(:x_neg => boundary,
-                           :x_pos => boundary,
-                           :y_neg => boundary_condition_slip_wall,
-                           :y_pos => boundary)
+boundary_conditions = (; x_neg = boundary,
+                       x_pos = boundary,
+                       y_neg = boundary_condition_slip_wall,
+                       y_pos = boundary)
 
 polydeg = 3
 basis = LobattoLegendreBasis(polydeg)

examples/euler/dry_air/tests/elixir_gemein_source_terms.jl

@@ -21,10 +21,11 @@ coordinates_max = (2.0, 2.0)
 
 cells_per_dimension = (16, 16)
 
-mesh = StructuredMesh(cells_per_dimension, coordinates_min, coordinates_max)
+mesh = StructuredMesh(cells_per_dimension, coordinates_min, coordinates_max, periodicity = true)
 
 semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition, solver,
-                                    source_terms = source_terms_convergence_test_dry)
+                                    source_terms = source_terms_convergence_test_dry,
+                                    boundary_conditions = boundary_condition_periodic)
 
 ###############################################################################
 # ODE solvers, callbacks etc.

examples/euler/dry_air/tests/elixir_potential_temperature_ec.jl

@@ -23,9 +23,11 @@ coordinates_min = (0.0,)
 coordinates_max = (1.0,)
 mesh = TreeMesh(coordinates_min, coordinates_max,
                 initial_refinement_level = 3,
-                n_cells_max = 100_000)
+                n_cells_max = 100_000,
+                periodicity = true)
 
-semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_density_wave, solver)
+semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_density_wave, solver,
+                                    boundary_conditions = boundary_condition_periodic)
 ###############################################################################
 # ODE solvers, callbacks etc.
 tspan = (0.0, 0.4)

examples/euler/dry_air/tests/elixir_potential_temperature_linear_hydrostatic.jl

@@ -104,10 +104,10 @@ linear_hydrostatic_setup = HydrostaticSetup(alpha, xr_B, equations)
 
 boundary = BoundaryConditionDirichlet(linear_hydrostatic_setup)
 
-boundary_conditions = Dict(:x_neg => boundary,
-                           :x_pos => boundary,
-                           :y_neg => boundary_condition_slip_wall,
-                           :y_pos => boundary)
+boundary_conditions = (; x_neg = boundary,
+                       x_pos = boundary,
+                       y_neg = boundary_condition_slip_wall,
+                       y_pos = boundary)
 
 # We have an isothermal background state with T0 = 250 K.
 # The reference speed of sound can be computed as:

examples/euler/dry_air/tests/elixir_potential_temperature_linear_nonhydrostatic.jl

@@ -101,10 +101,10 @@ linear_hydrostatic_setup = NonHydrostaticSetup(alpha, xr_B)
 
 boundary = BoundaryConditionDirichlet(linear_hydrostatic_setup)
 
-boundary_conditions = Dict(:x_neg => boundary,
-                           :x_pos => boundary,
-                           :y_neg => boundary_condition_slip_wall,
-                           :y_pos => boundary)
+boundary_conditions = (; x_neg = boundary,
+                       x_pos = boundary,
+                       y_neg = boundary_condition_slip_wall,
+                       y_pos = boundary)
 polydeg = 3
 basis = LobattoLegendreBasis(polydeg)
 surface_flux = (FluxLMARS(340.0), flux_zero)

examples/euler/dry_air/tests/elixir_potential_temperature_taylor_green_vortex.jl

@@ -30,7 +30,7 @@ mesh = StructuredMesh(cells_per_dimension, coordinates_min, coordinates_max,
                       periodicity = (true, true, true))
 
 semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_taylor_green_vortex,
-                                    solver)
+                                    solver, boundary_conditions = boundary_condition_periodic)
 ###############################################################################
 # ODE solvers, callbacks etc.
 tspan = (0.0, 0.2)

examples/euler/dry_air/tests/elixir_potential_temperature_well_balanced.jl

@@ -1,6 +1,6 @@
 # References:
 # - Marco Artiano, Oswald Knoth, Peter Spichtinger, Hendrik Ranocha (2025)
-#   Structure-Preserving High-Order Methods for the Compressible Euler Equations 
+#   Structure-Preserving High-Order Methods for the Compressible Euler Equations
 #   in Potential Temperature Formulation for Atmospheric Flows
 #   https://arxiv.org/abs/2509.10311 (pre-print)
 using OrdinaryDiffEqSSPRK
@@ -50,8 +50,10 @@ mesh = TreeMesh(coordinates_min, coordinates_max,
                 initial_refinement_level = 3,
                 n_cells_max = 100_000, periodicity = false)
 
-boundary_conditions = (x_pos = boundary_condition_slip_wall,
-                       x_neg = boundary_condition_slip_wall)
+boundary_conditions = (; x_pos = boundary_condition_slip_wall,
+                       x_neg = boundary_condition_slip_wall,
+                       y_pos = boundary_condition_slip_wall,
+                       y_neg = boundary_condition_slip_wall)
 
 semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_adiabatic, solver,
                                     boundary_conditions = boundary_conditions)

examples/euler/dry_air/tests/elixir_potential_temperature_well_balanced_curvilinear.jl

@@ -1,6 +1,6 @@
 # References:
 # - Marco Artiano, Oswald Knoth, Peter Spichtinger, Hendrik Ranocha (2025)
-#   Structure-Preserving High-Order Methods for the Compressible Euler Equations 
+#   Structure-Preserving High-Order Methods for the Compressible Euler Equations
 #   in Potential Temperature Formulation for Atmospheric Flows
 #   https://arxiv.org/abs/2509.10311 (pre-print)
 using OrdinaryDiffEqSSPRK
@@ -55,10 +55,10 @@ mesh = P4estMesh(trees_per_dimension, polydeg = polydeg,
                  mapping = mapping, periodicity = (false, false),
                  initial_refinement_level = 0)
 
-boundary_conditions = Dict(:x_pos => boundary_condition_slip_wall,
-                           :x_neg => boundary_condition_slip_wall,
-                           :y_pos => boundary_condition_slip_wall,
-                           :y_neg => boundary_condition_slip_wall)
+boundary_conditions = (; x_pos = boundary_condition_slip_wall,
+                       x_neg = boundary_condition_slip_wall,
+                       y_pos = boundary_condition_slip_wall,
+                       y_neg = boundary_condition_slip_wall)
 
 semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition_adiabatic, solver,
                                     boundary_conditions = boundary_conditions)

examples/euler/moist_air/buoyancy/elixir_hoeck_bubble.jl

@@ -28,7 +28,7 @@ end
 
 equations = CompressibleRainyEulerEquations2D()
 
-boundary_conditions = (x_neg = boundary_condition_periodic,
+boundary_conditions = (; x_neg = boundary_condition_periodic,
                        x_pos = boundary_condition_periodic,
                        y_neg = boundary_condition_slip_wall,
                        y_pos = boundary_condition_slip_wall)

examples/euler/moist_air/tests/elixir_gemein_source_terms.jl

@@ -30,10 +30,11 @@ coordinates_max = (2.0, 2.0)
 
 cells_per_dimension = (4, 4)
 
-mesh = StructuredMesh(cells_per_dimension, coordinates_min, coordinates_max)
+mesh = StructuredMesh(cells_per_dimension, coordinates_min, coordinates_max, periodicity = true)
 
 semi = SemidiscretizationHyperbolic(mesh, equations, initial_condition, solver,
-                                    source_terms = source_terms_convergence_test_moist)
+                                    source_terms = source_terms_convergence_test_moist,
+                                    boundary_conditions = boundary_condition_periodic)
 
 ###############################################################################
 # ODE solvers, callbacks etc.

examples/euler/precipitation/buoyancy/elixir_hoeck_bubble.jl

@@ -26,7 +26,7 @@ end
 ###############################################################################
 # semidiscretization of the compressible rainy Euler equations
 
-boundary_conditions = (x_neg = boundary_condition_periodic,
+boundary_conditions = (; x_neg = boundary_condition_periodic,
                        x_pos = boundary_condition_periodic,
                        y_neg = boundary_condition_simple_slip_wall,
                        y_pos = boundary_condition_simple_slip_wall)

examples/euler/precipitation/buoyancy/elixir_hoeck_bubble_diffusion.jl

@@ -30,12 +30,12 @@ end
 diffusivity = 0.5f0
 equations_parabolic = LaplaceDiffusion2D(diffusivity, equations)
 
-boundary_conditions = (x_neg = boundary_condition_periodic,
+boundary_conditions = (; x_neg = boundary_condition_periodic,
                        x_pos = boundary_condition_periodic,
                        y_neg = boundary_condition_simple_slip_wall,
                        y_pos = boundary_condition_simple_slip_wall)
 
-boundary_conditions_parabolic = (x_neg = boundary_condition_periodic,
+boundary_conditions_parabolic = (; x_neg = boundary_condition_periodic,
                                  x_pos = boundary_condition_periodic,
                                  y_neg = boundary_condition_laplace,
                                  y_pos = boundary_condition_laplace)